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Lake Pocotopaug Lake and Watershed Restoration Evaluation ...

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elow 7:1 occurred on September 22, 1993 at surface <strong>and</strong> mid depths <strong>and</strong> occurred in May,August, <strong>and</strong> September in 1993 at the bottom.The trophic state of <strong>Lake</strong> <strong>Pocotopaug</strong>, determined as Carlson’s (1977) trophic state index (TSI)from July <strong>and</strong> August SDT, surface TP, <strong>and</strong> chlorophyll a (chl a) values was typical ofmesotrophic conditions (intermediate nutrient levels) during summer stratification. TSI valueshigher than 60 are indicative of degraded (eutrophic) conditions, while TSI values below 40typically apply to oligotrophic lakes (Carlson 1977). Mitchell (2000) proposes a TSI=70threshold for contact recreation. TSI for all categories were below 60 but above 40.Using July <strong>and</strong> August data from 1991-2001, the trophic state of <strong>Lake</strong> <strong>Pocotopaug</strong>, asdetermined from the State of Connecticut Water Quality St<strong>and</strong>ards, is mesotrophic,(intermediate nutrient levels). Table 11 compares <strong>Lake</strong> <strong>Pocotopaug</strong> range of means with StateWater Quality St<strong>and</strong>ards for mesotrophic conditions.Table 11. <strong>Lake</strong> <strong>Pocotopaug</strong> July <strong>and</strong> August Range of Annual Means <strong>and</strong> Water QualitySt<strong>and</strong>ards for Mesotrophic <strong>Lake</strong>s in Connecticut.Mesotrophic St<strong>and</strong>ard <strong>Lake</strong> <strong>Pocotopaug</strong>Annual Mean Range(July <strong>and</strong> August)TP 10-30 ug/L spring <strong>and</strong> summer 11-23TN 200-600 ug/L spring <strong>and</strong> summer 440Chl a 2-15 ug/L mid summer 5.5-7.4SDT 2-6 meters mid summer 0.7-3.5Dissolved iron provides a measure of the potential of a water body to limit phosphorus internalloading. Ferrous iron (Fe ++ ) is often released from anoxic sediments along with dissolvedphosphorus (DP). Ferric iron (Fe +++ ) is the dominant form of iron in the presence of oxygen, <strong>and</strong>forms from Fe ++ . Iron tends to bind with phosphorus during this conversion <strong>and</strong>, because of lowsolubility, iron phosphates precipitate to the sediment.Dissolved iron concentrations just above the water-sediment interface provide a measure of thepotential for release of sediment-bound phosphorus <strong>and</strong> its return to the sediments. Dissolvediron values much higher than 1.0 mg/l are often indicative of substantial redox activity in thesediments, whereby chemical oxidation-reduction reactions can allow certain contaminants tobe released from the sediment back into the water column. However, dissolved iron in excessof ten times the DP level is usually sufficient to precipitate out all DP under oxic conditions, sophosphorus released by this mechanism will not necessarily be available for algal uptake <strong>and</strong>growth.<strong>Lake</strong> <strong>Pocotopaug</strong> <strong>Restoration</strong> <strong>Evaluation</strong> 38May 2002

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